玻化微珠级配对玻化微珠保温混凝土性能的影响

为了选定最优的玻化微珠级配,在 C35玻化微珠保温混凝土配合比的基础上,选用6种不同级配的玻化微珠制成6组保温混凝土,分析保温混凝土的坍落度、离析与泌水情况、抗压强度和导热系数。结果表明：随着玻化微珠级配的减小,玻化微珠的容重越来越大;保温混凝土的坍落度越来越小,经时损失不断增大,流动性比较差,无离析和泌水现象,黏聚性和保水性良好,抗压强度越来越大,导热系数先减少后增加。最终选用的玻化微珠的级配为1．5～3．5 mm,容重为85～90 g／L。     

自保温再生混凝土的配合比优化设计

研究了不同再生细骨料取代率和玻化微珠体积掺量对再生保温混凝土性能的影响.对28 d龄期各组试块的立方体抗压强度、导热系数和密度进行了测试,对试验结果进行了分析,综合28 d立方体抗压强度和导热系数两个指标对自保温再生混凝土的配合比进行了优化.结果表明:随玻化微珠体积掺量增加,28 d立方体抗压强度、导热系数和密度均降低;再生细骨料取代率和玻化微珠体积掺量同28 d立方体抗压强度、导热系数和密度的关系可由多项式拟合;再生细骨料取代率为50%、玻化微珠体积掺量为110%时的配合比为优化配合比.     

引气型玻化微珠粉煤灰保温混凝土抗压强度和导热系数试验研究

以玻化微珠和粉煤灰为变量,测试引气型保温混凝土的力学性能和热工性能.试验结果表明:引气型玻化微珠粉煤灰保温混凝土抗压强度数值区间为13.9～35.4MPa,导热系数数值区间为0.371～0.432W/(m·K);抗压强度与导热系数呈现相同的变化规律;随玻化微珠和粉煤灰掺量的递增,混凝土抗压强度与导热系数呈现先增大后降低的变化规律;当玻化微珠掺量为20%和粉煤灰掺量为10%时,保温混凝土抗压强度为35.4 MPa,导热系数为0.432 W/(m·K),同时满足承重与保温一体化的双向性能要求.     

秸秆/聚丙烯纤维-玻化微珠保温混凝土抗冻融试验研究

为探索冻融循环下秸秆粉末、聚丙烯纤维和玻化微珠对保温混凝土导热性能的影响,采用正交试验设计16组保温混凝土并进行抗压强度、抗拉强度和导热系数的试验测试,分析秸秆粉末体积率(因素A)、玻化微珠代砂体积率(因素B)、聚丙烯纤维体积率(因素C)对秸秆/聚丙烯纤维-玻化微珠保温混凝土导热系数变化和质量损失的影响。结果表明,随冻融循环次数增加,混凝土隔热能力和质量均不断降低;80次冻融循环后导热系数平均增大49.97%,质量损失平均降低37.93%。极差分析表明,对导热系数的影响顺序为：因素A>因素B>因素C,对质量损失的影响顺序为：因素A>因素C>因素B。冻融循环下,秸秆纤维对保温混凝土导热系数、质量损失的影响较其他掺合料明显,并可有效延长热量传递路径,提高保温效果。     

引气型玻化微珠粉煤灰保温混凝土性能试验研究

以轻集料玻化微珠和工业废弃物粉煤灰制备引气型玻化微珠粉煤灰保温混凝土﹒利用正交试验方法,测试玻化微珠和粉煤灰在不同掺量下引气型玻化微珠粉煤灰保温混凝土的抗压强度和劈裂抗拉强度,得出其最优掺量,并测定该掺量下混凝土试件的导热系数﹒试验结果表明:当玻化微珠掺量为20%、粉煤灰掺量为10%时,引气型玻化微珠粉煤灰保温混凝土抗压强度为35.4MPa,劈裂抗拉强度为2.15MPa,导热系数为0.431 73 W/(m·K),力学性能和热工性能均能达到我国建筑墙体材料的设计标准,满足建筑节能需求﹒     

不同替代率再生混凝土基本性能试验

为研究再生混凝土的基本性能,选用替代率分别为30%、50%、80%、100%,基本水灰质量分数比为0.40、0.50,砂率为30%等条件下的再生粗骨料混凝土为研究对象,通过试验观察和数据分析,得出以下结论:在水灰质量分数比和砂率相同的条件下,不同替代率的再生混凝土的流动性和抗压强度均比普通混凝土差,且除100%再生混凝土外,其他再生混凝土的强度随着再生骨料取代率的增加而逐渐降低;当再生骨料替代率≤50%时,再生混凝土的粘聚性和保水性都满足要求;而替代率50%时,其流动性、保水性、粘聚性都较差;在替代率和水灰质量分数比都较高的条件下,提高砂率能有效改善再生混凝土的和易性.建议再生混凝土表观密度取值为(2 400±100)kg/m3.     

不同水胶比对玻化微珠保温砂浆性能的影响

研究了当水胶比分别为1.2,1.3,1.4和1.5时,玻化微珠保温砂浆的干燥收缩、抗压强度、抗折强度、干密度、导热系数等性能指标.通过压汞试验和SEM扫描电镜分析,从微观角度进一步揭示了玻化微珠保温砂浆的性能指标随水胶比变化的原因.试验结果表明:玻化微珠保温砂浆的干燥收缩随着水胶比的增大呈现明显增大的趋势;当水胶比一定时,玻化微珠保温砂浆的干燥收缩早期增长速率较快,后期增长速率较慢;当水胶比分别为1.3,1.4和1.5时,玻化微珠保温砂浆的抗压强度、抗折强度、干密度、导热系数与水胶比为1.2时相比均有了较为明显的变化,抗压强度分别下降了13.1%,40.0%和73.8%;抗折强度分别下降了18.8%,35.7%和77.7%;干密度分别减小了8.3%,19.4%和33.3%;导热系数也分别下降了4.6%,11.3%和21.4%.玻化微珠保温砂浆的各项性能随着水胶比的变化,产生了明显的变化.通过压汞试验和SEM分析发现,随着水胶比的增大,玻化微珠保温砂浆内部孔隙增多.     

玻化微珠对纳米保温混凝土抗压强度分布特征影响

通过使用太原理工大学实验室的DYE—2000数字压力试验机对294块立方体试块做抗压强度试验,主要研究了玻化微珠含量分别为30%、70%、130%(体积分数)的纳米玻化微珠保温承重混凝土抗压强度及概率分布特征。根据试验数据,得到了不同玻化微珠含量的纳米玻化微珠保温承重混凝土抗压强度的均值、标准差以及变异系数;同时通过正态分布模型对纳米玻化微珠保温承重混凝土的抗压强度的分布进行了检验;研究表明,不同玻化微珠含量对纳米玻化微珠保温承重混凝土抗压强度的变异系数影响不大;当显著性水平α=0.05时,可以用正态分布模型描述不同玻化微珠含量的纳米玻化微珠保温承重混凝土抗压强度的概率分布规律;最后根据统计分析和Bayes估计的结果,对C30纳米玻化微珠保温承重混凝土抗压强度的标准差给出了建议取值。     

玻化微珠保温混凝土的抗折强度试验研究

为了研究玻化微珠保温混凝土的抗折强度,设计了玻化微珠保温混凝土和普通混凝土抗折试验标准试件,并对折断后的玻化微珠保温混凝土抗折试件进行抗压试验,获取同一试件的立方体抗压强度。分析了玻化微珠保温混凝土的抗折破坏形态,回归了玻化微珠保温混凝土抗折强度与立方体抗压强度的经验关系式。试验与分析结果表明:玻化微珠保温混凝土与普通混凝土的抗折破坏形态基本一致,破坏均为粗骨料与水泥浆凝胶体间的粘结破坏;玻化微珠保温混凝土的抗折强度略高于普通混凝土;玻化微珠保温混凝土抗折强度与抗压强度关系式可为玻化微珠保温混凝土的结构设计提供理论参考。     

玻化微珠保温混凝土抗压强度与导热系数研究

随着全球能源危机的日益加剧和我国节能减排等相关政策的大力推行,开发研制节能型的新的建筑结构体系成为土木工程领域的重要课题。提出了一种新型保温混凝土——玻化微珠保温混凝土,该混凝土是一种既具有一般混凝土的物理力学性能,同时又具有保温性能、绿色、环保的高效益生态建筑材料。通过混凝土的正交试验,分析了相关因素对混凝土的导热系数和抗压强度的影响规律,验证了在混凝土中掺加一定数量的玻化微珠配制玻化微珠保温混凝土的可行性。     

Markedness and its Interpretation in Language Use

Language markedness is a common phenomenon in languages, and is reflected from hearing, vision and sense, i.e. the variation in the three aspects such as phonology, morphology and semantics. This paper focuses on the interpretation of markedness in language use following the three perspectives, i.e. pragmatic interpretation, psychological interpretation and cognitive interpretation, with an aim to define the function of markedness.     

Lower Paleozoic oil relationships within Williston Basin, Canada

The Williston Basin is a significant petroleum province, containing oil production zones that include the Middle Cambrian to Lower Ordovician, Upper Ordovician, Middle Devonian, Upper Devonian and Mississippian and within the Jurassic and Cretaceous. The oils of the Williston Basin exhibit a wide range of geochemical characteristics defined as "oil families", although the geochemical signature of the Cambrian Deadwood Formation and Lower Ordovician Winnipeg reservoired oils does not match any "oil family". Despite their close stratigraphic proximity, it is evident that the oils of the Lower Palaeozoic within the Williston Basin are distinct. This suggests the presence of a new "oil family" within the Williston Basin. Diagnostic geochemical signatures occur in the gasoline range chromatograms, within saturate fraction gas chromatograms and biomarker fingerprints. However, some of the established criteria and cross-plots that are currently used to segregate oils into distinct genetic families within the basin do not always meet with success, particularly when applied to the Lower Palaeozoic oils of the Deadwood and Winnipeg Formation.     

An Analysis of Catherine＇s Character——Wuthering Heights

Wuthering Heights, Emily Bronte＇s only novel, was published in December of 1847 under the pseudonym Ellis Bell. The book did not gain immediate success, but it is now thought one of the finest novels in the English language. Catherine is the key character of this masterpiece, because everybody and everything center on her though she had a short life. We can understand this masterpiece better if we know Catherine well.     

Features of Women's language

Language is a means of verbal communication. People use language to communicate with each other. In the society, no two speakers are exactly alike in the way of speaking. Some differences are due to age, gender, statue and personality. Above all, gender is one of the obvious reasons. The writer of this paper tries to describe the features of women＇s language from these perspectives： pronunciation, intonation, diction, subjects, grammar and discourse. From the discussion of the features of women＇s language, more attention should be paid to language use in social context. What＇s more, the linguistic phenomena in a speaking community can be understood more thoroughly.     

Characterization of Ordovician carbonate reservoirs, southeastern Saskatchewan, Canada

The discovery of the prolific Ordovician Red River reservoirs in 1995 in southeastern Saskatchewan was the catalyst for extensive exploration activity which resulted in the discovery of more than 15 new Red River pools. The best yields of Red River production to date have been from dolomite reservoirs. Understanding the processes of dolomitization is, therefore, crucial for the prediction of the connectivity, spatial distribution and heterogeneity of dolomite reservoirs.The Red River reservoirs in the Midale area consist of 3～4 thin dolomitized zones, with a total thickness of about 20 m, which occur at the top of the Yeoman Formation. Two types of replacement dolomite were recognized in the Red River reservoir: dolomitized burrow infills and dolomitized host matrix. The spatial distribution of dolomite suggests that burrowing organisms played an important role in facilitating the fluid flow in the backfilled sediments. This resulted in penecontemporaneous dolomitization of burrow infills by normal seawater. The dolomite in the host matrix is interpreted as having occurred at shallow burial by evaporitic seawater during precipitation of Lake Almar anhydrite that immediately overlies the Yeoman Formation. However, the low δ18O values of dolomited burrow infills (-5.9‰～ -7.8‰, PDB) and matrix dolomites (-6.6‰～ -8.1‰, avg. -7.4‰ PDB) compared to the estimated values for the late Ordovician marine dolomite could be attributed to modification and alteration of dolomite at higher temperatures during deeper burial, which could also be responsible for its 87Sr/86Sr ratios (0.7084～0.7088) that are higher than suggested for the late Ordovician seawaters (0.7078～0.7080). The trace amounts of saddle dolomite cement in the Red River carbonates are probably related to "cannibalization" of earlier replacement dolomite during the chemical compaction.     

Design and analysis of generic LBS application developing platform

Location based services is promising due to its novel working style and contents.A software platform is proposed to provide application programs of typical location based services and support new applications developing efficiently. The analysis shows that this scheme is easy implemented, low cost and adapt to all kinds of mobile nework system.     

橡胶颗粒沥青混合料低温抗裂性试验研究

以AC-13级配为基础,将橡胶颗粒代替部分集料掺入混合料中,以低温弯曲试验为评价方法对不同橡胶颗粒掺量下沥青混合料的低温抗裂性进行研究,并引入应变能密度值对混合料的低温抗裂性进行综合评价.试验结果表明:橡胶颗粒沥青混合料试件的破坏微应变均超过2 300,满足冬寒区的技术指标;无论是否掺加橡胶颗粒,随着温度的下降,沥青混合料破坏时的最大弯拉强度增大,弯拉应变降低,劲度模量增大;弯曲应变能密度在胶粒掺量为1%左右时具有较大的弯曲应变能密度值,此时橡胶颗粒沥青混合料具有较好的低温抗裂性.     

低渗透非均质砂岩油藏启动压力梯度研究

理论推导与室内实验相结合,建立了低渗透非均质砂岩油藏启动压力梯度确定方法。首先借助油藏流场与电场相似的原理,推导了非均质砂岩油藏启动压力梯度计算公式。其次基于稳定流实验方法,建立了非均质砂岩油藏启动压力梯度测试方法。结果表明:低渗透非均质砂岩油藏的启动压力梯度确定遵循两个等效原则。平面非均质油藏的启动压力梯度等于各级渗透率段的启动压力梯度关于长度的加权平均;纵向非均质油藏的启动压力梯度等于各渗透率层的启动压力梯度关于渗透率与渗流面积乘积的加权平均。研究成果可用于有效指导低渗透非均质砂岩油藏的合理井距确定,促进该类油藏的高效开发。     

On Tragic Consciousness In The Works By Ernest Hemingway

As an American modern novelist who were famous in the literary world, Hemingway was not a person who always followed the trend but a sharp observer. At the same time, he was a tragedy maestro, he paid great attention on existence, fate and end-result. The dramatis personae's tragedy of his works was an extreme limit by all means tragedy on the meaning of fearless challenge that failed. The beauty of tragedy was not produced on the destruction of life, but now this kind of value was in the impact activity. They performed for the reader about the tragedy on challenging for the limit and the death.     

Quantitative trait loci （QTLs） for quality traits related to protein and starch in wheat

Quality traits in wheat （Triticum aestirum L.） were studied by quantitative trait locus （QTL） analysis in a recombinant inbred line （RIL） population, a set of 131 lines derived from Chuan 35050 × Shannong 483 cross （ChSh）. Grains from RILs were assayed for 21 quality traits related to protein and starch. A total of 35 putative QTLs for 19 traits with a single QTL explaining 7.99-40.52% of phenotypic variations were detected on 10 chromosomes, 1D, 2A, 2D, 3B, 3D, 5A, 6A, 6B, 6D, and 7B. The additive effects of 30 QTLs were positive, contributed by Chuan 35050, the remaining 5 QTLs were negative with the additive effect contributed by Shannong 483. For protein traits, 15 QTLs were obtained and most of them were located on chromosomes 1 D, 3B and 6D, while 20 QTLs for starch traits were detected and most of them were located on chromosomes 3D, 6B and 7B. Only 7 QTLs for protein and starch traits were co-located in three regions on chromosomes 1D, 2A and 2D. These protein and starch trait QTLs showed a distinct distribution pattern in certain regions and chromosomes. Twenty-two QTLs were clustered in 6 regions of 5 chromosomes. Two QTL clusters for protein traits were located on chromosomes 1D and 3B, respectively, three clusters for starch traits on chromosomes 3D, 6B and 7B, and one cluster including protein and starch traits on chromosome 1D.